Phase Relations in Peridotitic and Pyroxenitic Rocks in the Model Systems CMASH and NCMASH
Phase Relations in Peridotitic and Pyroxenitic Rocks in the Model Systems CMASH and NCMASH
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DOI：
10.1093/petrology/41.1.69
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发表时间：
2000
影响因子：
3.9
通讯作者：
E. Schmädicke
中科院分区：
文献类型：
--
作者：
E. Schmädicke
被认为处于平衡状态的矿物相。对于橄榄岩和辉石岩，由于它们具有共同的高温印记和平衡良好的高变异矿物组合，
mineral phases thought to be in equilibrium. In the case of peridotite and pyroxenite, with their common hightemperature imprint and their well-equilibrated highvariance mineral assemblages, this method usually results